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  <front>
    <journal-meta>
      <journal-id journal-id-type="issn">2411-3336</journal-id>
      <journal-id journal-id-type="eissn">2541-9404</journal-id>
      <journal-title-group>
        <journal-title xml:lang="ru">Записки Горного института</journal-title>
        <journal-title xml:lang="en">Journal of Mining Institute</journal-title>
      </journal-title-group>
      <publisher>
        <publisher-name xml:lang="ru">Санкт-Петербургский горный университет императрицы Екатерины ΙΙ</publisher-name>
        <publisher-name xml:lang="en">Empress Catherine II Saint Petersburg Mining University</publisher-name>
      </publisher>
    </journal-meta>
    <article-meta>
      <article-id custom-type="edn" pub-id-type="custom">ROAVGE</article-id>
      <article-id custom-type="pmi" pub-id-type="custom">pmi-16309</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/16309</article-id>
      <article-categories>
        <subj-group subj-group-type="section-heading" xml:lang="ru">
          <subject>Геотехнология и инженерная геология</subject>
        </subj-group>
        <subj-group subj-group-type="section-heading" xml:lang="en">
          <subject>Geotechnical Engineering and Engineering Geology</subject>
        </subj-group>
      </article-categories>
      <title-group>
        <article-title xml:lang="en">Geochemical studies of rocks of the Siberian igneous province and their role in the formation theory of unique platinum-copper-nickel deposits</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Геохимические исследования пород Сибирской магматической провинции и их роль в теории образования уникальных платино-медно-никелевых месторождений</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Krivolutskaya</surname>
            <given-names>Nadezhda А.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Криволуцкая</surname>
              <given-names>Н. А.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Krivolutskaya</surname>
              <given-names>Nadezhda А.</given-names>
            </name>
          </name-alternatives>
          <email>nakriv@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0002-5709-7785</contrib-id>
          <xref ref-type="aff" rid="aff1"/>
        </contrib>
        <aff-alternatives id="aff1">
          <aff>
            <institution xml:lang="ru">Институт геохимии и аналитической химии им. В.И.Вернадского РАН (Москва, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">V.I.Vernadsky Institute of Geochemistry and Analytical Chemistry of RAS (Moscow, Russia)</institution>
          </aff>
        </aff-alternatives>
      </contrib-group>
      <pub-date pub-type="epub" iso-8601-date="2024-04-23">
        <day>23</day>
        <month>04</month>
        <year>2024</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>2024</year>
      </pub-date>
      <volume>269</volume>
      <fpage>738</fpage>
      <lpage>756</lpage>
      <history>
        <date date-type="received" iso-8601-date="2023-08-31">
          <day>31</day>
          <month>08</month>
          <year>2023</year>
        </date>
        <date date-type="accepted" iso-8601-date="2023-12-27">
          <day>27</day>
          <month>12</month>
          <year>2023</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="2024-11-12">
          <day>12</day>
          <month>11</month>
          <year>2024</year>
        </date>
      </history>
      <permissions>
        <copyright-statement>© Nadezhda А. Krivolutskaya</copyright-statement>
        <copyright-year>2024</copyright-year>
        <copyright-holder xml:lang="ru">Н. А. Криволуцкая</copyright-holder>
        <copyright-holder xml:lang="en">Nadezhda А. Krivolutskaya</copyright-holder>
        <license xlink:href="http://creativecommons.org/licenses/by/4.0">
          <license-p>CC BY 4.0</license-p>
        </license>
      </permissions>
      <self-uri xlink:type="simple" xlink:href="https://pmi.spmi.ru/pmi/article/view/16309">https://pmi.spmi.ru/pmi/article/view/16309</self-uri>
      <abstract xml:lang="ru">
        <p>Норильские месторождения, уникальные как по геологическому строению, так и запасам никеля и платиновых металлов, привлекают внимание исследователей на протяжении нескольких десятилетий. Было предложено несколько гипотез их образования, из которых наибольшее распространение получили две: модель формирования руд в промежуточной камере и внедрение обогащенного сульфидами пикритового расплава на место кристаллизации и образование сульфидов in situ за счет ассимиляции толеитовой магмой сульфатсодержащих осадков при ее движении к поверхности. Главными вопросами генезиса в этих построениях являются состав родоначальных магм рудоносных массивов; взаимоотношение интрузивных и эффузивных пород; масштаб и роль ассимиляции вмещающих пород магмами. Эти вопросы рассматриваются в статье на примере большого объема аналитических данных, полученных автором при исследовании геологического строения магматических образований Норильского района. На их основании сделан вывод о том, что ни одна из предложенных моделей полностью не объясняет наблюдаемые факты, а также появление уникальных сульфидных руд. Для решения проблемы генезиса норильских месторождений необходим анализ развития P3-T1 магматизма во времени на территории всей крупной Сибирской магматической провинции, особенно ее восточной части, и установление связи с ним процессов рудообразования. Важнейшую роль в генезисе месторождений играло развитие Енисей-Хатангского прогиба, установление эволюции которого является первоочередной задачей в образовании сульфидных руд. Ее решение должно во многом базироваться наряду с геофизическими данными на изучении геохимии магматических пород провинции.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>The Norilsk deposits, unique both in their geological structure and reserves of nickel and platinum, have attracted the attention of researchers for several decades. Several hypotheses have been proposed to explain their formation. Two of them are the most widely accepted: the model of ore formation in an intermediate chamber from picritic melt enriched in sulphides and the formation of sulphides in situ through the assimilation of sulphate-bearing sediments by tholeiitic magma as it rises to the surface. The main questions regarding the genesis of these deposits are: the composition of the parental magmas that formed the ore-bearing massifs; the relationship between intrusions and effusive rocks; and the extent and role of assimilation of host rocks by magmas. These issues are discussed in the article using a large amount of analytical data obtained by the author during the study of the magmatic rocks and geological structures in the Norilsk area. Based on these data, it was concluded that none of the proposed models could fully explain all observed geological features of the deposits as well as the appearance of the unique sulphide ores. In order to solve the problem of the genesis of the Norilsk deposits, it is necessary to analyse the evolution of P3-T1 magmatism over time in the Siberian large igneous province, especially in its eastern part, and to determine its association with ore-forming processes; and its investigating it is a priority task for understanding sulphide ore formation. Solving this task should be based not only on geophysical data but also on studies of the geochemistry of igneous rocks within the province.</p>
      </abstract>
      <kwd-group xml:lang="ru">
        <title>Ключевые слова</title>
        <kwd>Норильский район</kwd>
        <kwd>Cu-Ni месторождения</kwd>
        <kwd>Сибирская провинция</kwd>
        <kwd>магматические породы</kwd>
        <kwd>геохимия</kwd>
      </kwd-group>
      <kwd-group xml:lang="en">
        <title>Keywords</title>
        <kwd>Norilsk region</kwd>
        <kwd>Cu-Ni deposits</kwd>
        <kwd>Siberian province</kwd>
        <kwd>igneous rocks</kwd>
        <kwd>geochemistry</kwd>
      </kwd-group>
      <funding-group>
        <funding-statement xml:lang="ru">Работа выполнена при финансовой поддержке Минобрнауки РФ №  13.1902.21.0018 (соглашение 075-15-2020-802).</funding-statement>
        <funding-statement xml:lang="en">The work was carried out with financial support from the Ministry of Education and Science of the RF N 13.1902.21.0018 (agreement 075-15-2020-802).</funding-statement>
      </funding-group>
    </article-meta>
  </front>
  <body/>
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